Silfra

Silfra fissure.
The Mid-Atlantic Ridge passing through Þingvellir

Silfra is a rift formed in the divergent tectonic boundary between the North American and Eurasian plates and is located in the Þingvallavatn Lake in the Þingvellir National Park in Iceland.

Formation

Silfra lies in the Þingvellir valley and within the Þingvellir National Park. The valley, and Silfra itself, were formed by the divergent tectonic drift of the Eurasian and North American plates. The plates drift about 2 cm farther apart every year, building up tension between the plates and the earth mass above. This tension is relieved through periodic major earthquakes at approximately ten year intervals, which have caused cracks and fissures to form in Þingvellir valley; Silfra lies at the rim of the Þingvallavatn Lake [1] and is one of the largest and deepest of these fissures. The Silfra fissure intercepts a major aquifer, which feeds multiple springs at its base.[2] Boulders and rocks falling into the widening cracks have formed caves within the fissures.[1][3]

Hydrology

Silfra is spring fed by groundwater originating as meltwater from Langjökull, Iceland's second largest glacier, about fifty kilometres north of the Þingvallavatn Lake. In the distant past, this Langjökull meltwater ran through a river directly and unimpeded into the Þingvallavatn Lake. This river was blocked a few thousand years ago by lava flows from the Skjaldbreiður volcano causing the meltwater to pond and seep underground into the porous lava rock to form an aquifer. This water then percolates through the aquifer for thirty to a hundred years before emerging from the fissure springs in the Þingvallavatn Lake fifty kilometres to the south. The emerging, highly filtered, groundwater is exceptionally clear and potable.[2][4][5]

Scuba diving

The diver's right hand is on the North American Plate and the left hand on the Eurasian Plate

Scuba divers and snorkelers are attracted to Sifra's exceptionally clear, fresh, water, its geological significance and the rare opportunity to swim between continental plates.[6][7][8] The rift offers exceptional visibility of 70–80 metres.. The site has been placed on the world's top fifty diving destinations by at least one travel site.[9]

There are three main dive sites: Silfra Hall, Silfra Cathedral and Silfra Lagoon. The most spectacular section is the Cathedral, which is a 100 metres long fissure with visibility almost from end to end.[10] Shallow at the entry points at the ends of the fissure, Silfra descends to a maximum depth of 63 metres but diving to this depth is seldom done as it requires technical diving skills. The water temperature is between 2–4 °C (36–39 °F) but can be comfortably dived using a dry suit.

See also

References

  1. 1 2 Geology of Silfra, Silfra.org – website
  2. 1 2 Water in Silfra, Silfra.org – website
  3. ↑ Silfra Caves, Silfra.org – website
  4. ↑ Top Diving Destination, Dive Iceland
  5. ↑ diveiceland.com http://www.diveiceland.com/index.php?page=silfra. Missing or empty |title= (help), diving Video of Silfra
  6. ↑ Detailed information and photos of Silfra, Silfra.org – website
  7. ↑ Diving, Þingvellir National Park website
  8. ↑ Detailed description of Silfra, DIVE.IS website
  9. ↑ Into the deep: World’s 50 best dive sites, CNN Travel
  10. ↑ Three sections of Silfra, Total Iceland

Coordinates: 64°15′18″N 21°07′23″W / 64.255°N 21.123°W / 64.255; -21.123

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